1. Angle of incidence, the angle at which the sun rays from the sun strike earth's surface.if the rays strike the earth at angle less than 90 degrees the energy spread over large portion of the earth. But when the ray strike at exactly 90 degrees the energy concentrate on small area.
2. Day leghth refers to the duration of the sunlight, longer days allows more insolation and more heat is absorbed.
3. Atmospheric obstruction;the longer the incident rays passes through the atmosphere the more the weaker the intensity of energy at the earth's surface.
4. latitudinal sunshift.sun rays normally shift from northward and southwards during the course of the year.therefore low latitude receive surplus energy with more coming energy than outgoing energy
The amount of sunlight received by anywhere on the planet is influenced primarily by two factors: altitude and latitude. The deeper one is in the atmosphere (i.e. the closer one is to sea level) the more atmosphere there is to scatter the incoming light from the sun. Thus, at higher elevations, the light concentration received by the ground is closer to the actual amount emitted by the sun. Latitude, on the other hand, affects sunlight because of the geometry of the planet. Since Earth is an oblate spheroid, if a cylinder of light were to shine straight down on it, the shape that would appear on the surface would be circular. However, as the angle of inclination decreases, this shape starts to turn elliptical. Thus, the same "volume" of light is shining over a wider surface area and so the light is less concentrated. Basically, higher altitude, lower latitude areas receive a great amount of sunlight, while lower altitude, higher latitude areas receive a comparatively small amount.
The amount of solar energy absorbed at the Earth's surface is most influenced by factors such as the angle and intensity of sunlight, the presence of clouds, air pollution, and surface properties like albedo (reflectivity) and vegetation cover. These factors determine how much sunlight reaches and is absorbed by the surface.
The unequal heating of the Earth's surface is caused by factors such as the angle of incidence of sunlight, atmospheric circulation patterns, and the distribution of land and water. This leads to variations in temperature and weather patterns across different regions of the planet.
Thick cloud cover can act as a blanket, trapping heat and causing the surface temperature to increase. Conversely, it can also reflect sunlight back into space, leading to a cooling effect on the surface temperature. The net effect depends on factors such as cloud altitude, composition, and thickness.
The amount of energy absorbed or reflected by Earth's surface depends on characteristics like surface color, texture, albedo (reflectivity), cloud cover, atmospheric composition, latitude, season, and time of day. These factors influence how much sunlight is absorbed or reflected by the surface, affecting the overall energy balance of the Earth.
Three factors that cause the amount of solar energy to vary over Earth's surface are the angle of sunlight, atmospheric conditions such as clouds and air pollution, and the duration of daylight hours.
The amount of sunlight reaching a location at a particular time is determined by Earth's shape, axial tilt, rotation, and orbit around the sun. These factors affect the angle at which sunlight hits the Earth's surface, leading to variations in day length and intensity of sunlight throughout the year.
The amount of solar energy absorbed at the Earth's surface is most influenced by factors such as the angle and intensity of sunlight, the presence of clouds, air pollution, and surface properties like albedo (reflectivity) and vegetation cover. These factors determine how much sunlight reaches and is absorbed by the surface.
i belive so
they affect by the sand
they obviously destroy things...
commonly 'sunlight', but more specifically UltraViolet radiation
The rotation of the Earth does not affect Earth's climate zones, as they are primarily influenced by factors such as sunlight intensity, ocean currents, and the distribution of land and water.
The unequal heating of the Earth's surface is caused by factors such as the angle of incidence of sunlight, atmospheric circulation patterns, and the distribution of land and water. This leads to variations in temperature and weather patterns across different regions of the planet.
It would block out significant sunlight, lowering the temperature.
The tectonic plates combined together
It blocks (some of) it from reaching the surface of the Earth.
The Earth may shift downward and may cause great damage.